Plates Moving Apart Types of Boundaries

Plates Moving Apart Types of Boundaries

PLATE TECTONICS IS The theory that the Earth s crust is broken into slabs of rock that move around on top of the asthenosphere.

How fast are plates moving? The Arctic Ridge has the slowest rate (less than 2.5 cm/yr) East Pacific Rise near Easter Island, in the South Pacific about 3,400 km west of Chile, has the fastest rate (more than 15 cm/yr).

How can the plates move? The plates can move away from each other Divergent towards each other Convergent or slide past each other Transform

PLATE MOTION Three types of plate boundary

DIVERGENT PLATE BOUNDARY Occur along spreading centers where plates are moving apart New crust is created by magma pushing up from the mantle

Mid-ocean ridges demonstrate that the ocean floor is spreading. The newer crust is in the center of the ocean. The continents are getting farther apart.

Divergent Boundary

Example: Mid-Atlantic Ridge A topographically high area near the middle of the Atlantic Ocean Splits the Atlantic Ocean, north to south,

Divergent: Atlantic Ridge LAVA FOUNTAINS KRAFLA VOLCANO ICELAND

Divergent: East African Rift Valley Three plates are moving away from each other. Area of seismic and volcanic activity.

Transform Boundaries Transform Boundaries occur where two plates are sliding past each other. These areas have large amounts of seismic activity due to plate motion.

Transform Boundary Earthquakes occur.

Example: San Andreas fault in California Pacific Plate slides past the North American Plate.

Convergent plate boundaries 3 types depending on type of plate involved: Oceanic-continental Oceanic-oceanic Continental-continental

Oceanic-Continental Collision Oceanic Nazca Plate is pushing into South American Plate. It is being subducted under the continental part of the South American Plate. South American Plate is being lifted up, creating the Andes Mountains. Strong, destructive earthquakes

Convergent Boundary

RING OF FIRE OCEANIC- CONTINENTAL Collisions cause most volcanic activity around the Pacific Ocean.

Nazca - S.America plate collision

Oceanic-oceanic Collision Subduction processes in oceanicoceanic plate convergence result in the formation of volcanic arc islands.

Island Arc Formation Oceanic- oceanic convergence: one plate subducted under the other plate. A trench is formed, example: Mariana trench. Erupted lava and volcanic debris pile up on the ocean floor until a submarine volcano rises above sea level to form an island volcano.

Continental-Continental Collision Neither plate subducts because the continental rocks are relatively light. Like two colliding icebergs, plates resist downward motion.

HIMALAYAS collision between the Indian and Eurasian plates has pushed up the Himalayas and the Tibetan Plateau

EVEREST, FROM LOBUCHE

Divergent Boundary Convergent Boundary Transform Boundary

The plate travels over a fixed spot or weak area in the crust. Examples are Hawaii and Yellowstone Park. Hot Spots

Examples of volcanic arc islands Aleutians the Kuriles Japan, the Ryukyus, the Philippines Indonesia

Plate Boundaries Divergent Boundary moving Convergent Boundary moving Transform Fault Boundary moving sideways past each other apart together

Transform-fault boundary where the North American and Pacific plates are moving past each other. Example: San Andreas Fault in California

Plate Boundaries Review Places where plates move apart are called divergent boundaries. When continental plates diverge a rift valley is formed. When two oceanic plates converge what is created? an island arc and a trench The Appalachians formed mainly from continental plate collisions and therefore are a folded mountain range. The force moving the plates is Convection currents.